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Modelling Hydrological Consequences of Climate Change-Progress and Challenges


doi: 10.1007/BF02918679

  • The simulation of hydrological consequences of climate change has received increasing attention from the hydrology and land-surface modelling communities. There have been many studies of climate-change effects on hydrology and water resources which usually consist of three steps: (1) use of general circulation models (GCMs) to provide future global climate scenarios under the effect of increasing greenhouse gases,(2) use of downscaling techniques (both nested regional climate models, RCMs, and statistical methods)for "downscaling" the GCM output to the scales compatible with hydrological models, and (3) use of hydrologic models to simulate the effects of climate change on hydrological regimes at various scales.Great progress has been achieved in all three steps during the past few years, however, large uncertainties still exist in every stage of such study. This paper first reviews the present achievements in this field and then discusses the challenges for future studies of the hydrological impacts of climate change.
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Manuscript History

Manuscript received: 10 November 2005
Manuscript revised: 10 November 2005
通讯作者: 陈斌, bchen63@163.com
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Modelling Hydrological Consequences of Climate Change-Progress and Challenges

  • 1. Department of Geosciences, University of Oslo, P. O. Box 1047 Blindern, N-0316 Oslo, Norvay;Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences,Department of Earth Sciences, Uppsala University, Villavagen 16, S-75236 Uppsala, Sweden,Department of Earth Sciences, Uppsala University, Villavagen 16, S-75236 Uppsala, Sweden

Abstract: The simulation of hydrological consequences of climate change has received increasing attention from the hydrology and land-surface modelling communities. There have been many studies of climate-change effects on hydrology and water resources which usually consist of three steps: (1) use of general circulation models (GCMs) to provide future global climate scenarios under the effect of increasing greenhouse gases,(2) use of downscaling techniques (both nested regional climate models, RCMs, and statistical methods)for "downscaling" the GCM output to the scales compatible with hydrological models, and (3) use of hydrologic models to simulate the effects of climate change on hydrological regimes at various scales.Great progress has been achieved in all three steps during the past few years, however, large uncertainties still exist in every stage of such study. This paper first reviews the present achievements in this field and then discusses the challenges for future studies of the hydrological impacts of climate change.

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